摘要
黔东松桃盘石—盘信地区经受了加里东期、印支期、燕山期等多期构造作用的改造,构造变形极为复杂。发育于湘黔两省的北东向慈利—保靖大型断裂为区内铅锌矿的重要导矿构造,为深源成矿流体的运移提供通道,其旁侧发育的一系列北东向、北北东向及北西向次级断裂常为重要的容矿空间。此外,受构造作用导致的节理裂隙、中小型皱褶尤其是背斜轴部等也是容矿的理想部位。
Panshi-Panxin region is located in Xuefeng western margin,East Songtao of Guizhou Province.The study area experienced Caledonian movement,Indosinian movement,Yanshan movement and their multiphase tectonic role transformation, tectonic deformation is very complex.Northeast to Cili-Baojing large fault is an important guide ore structure which development in Hunan and Guizhou Province,provide channels for deep source of ore-forming fluid migration, its side development of a series of NE, NNE and NW secondary fracture is often important ore space.In addition, the effect caused by structure joints and fissures, such as small and medium-sized ruffle especially anticline axis is the ideal place of hold ore.
作者
谢小峰
杨坤光
潘文
蒋天锐
钱山
袁良军
安正泽
Xie Xiaofeng;Yang Kunguang;Pan Wen;JiangTianrui;QianShan;Yuan Liang-jun;AnZhengze(School of Earth Sciences,China University of Geoscience,Wuhan,Hubei,430074,China;103 Geological Party,Guizhou Bureau of Geology ＆ Mineral Resources Tongren,Guizhou,554300,China;Hubei Earthquake Ageney,Wuhan,Hubei 430071,China)
出处
《化工矿产地质》
CAS
2018年第2期65-70,共6页
Geology of Chemical Minerals
基金
贵州省地质矿产勘查开发局地质科研专项项目"贵州松桃东部地区构造变形特征及其对铅锌矿的控制作用"(黔地矿科合(2015)01号)
中国地质调查局发展研究中心项目"贵州铜仁松桃锰矿整装勘查区矿产调查与找矿预测"(项目编号:121201004000160901-36)经费资助
关键词
铅锌矿
构造特征
盘石—盘信地区
贵州松桃东部
Lead-Zinc mine
tectonic characteristics
Panshi-Panxin region
Eastern Songtao of GuizhouProvince
